Kenya’s Rift Valley high levels a cause for concern
Recent high water levels of Kenya’s Rift Valley lakes have flooded properties and displaced communities, most notably around Lakes Baringo and Naivasha.
There are many lakes along the length of the African Rift Valley, which runs from the Red Sea in the north to Mozambique in the south. Kenya’s eastern Rift Valley has a string of eight lakes.
These lakes provide diverse habitats ranging from the freshwater lakes of Naivasha and Baringo to the semi-saline Lake Turkana, the saline alkaline lakes of Magadi, Elmentaita, Nakuru and Bogoria and the transient Lake Logipi.
The lake level rises are worrying because of the destruction to homes, livelihoods, industry and infrastructure, and loss of terrestrial wildlife habitat. So far this year, the rising waters of Lake Baringo alone have displaced more than 5,000 people and destroyed schools, hospitals, hotels and roads.
And the effects on lake ecologies are a concern as flooding increases lake turbidity and dilutes the saline waters of alkaline lakes.
The Rift Valley is subject to ongoing plate tectonics and crustal movement that can affect the lakes. The recent rises, though, are directly associated with above-average rainfall. The lakes have been even higher in the past, and with rainfall in the Rift Valley Basin being on a rising rainfall trend, higher lake levels can be expected in the future.
Land use changes, riparian zone encroachment, loss of wetlands, and urban growth are all contributing to more extreme flooding. This is because the proportion of rain and sediment that runs off from the catchments is increasing.
The lakes’ water cycles are governed by rainfall on highland catchment areas, evaporation and seepage. Water reaches the lakes through direct rainfall, rivers, groundwater flows, and in some cases hot springs from underground geothermal fields.
The eastern Rift Valley is semi-arid and its high evaporation rate concentrates salts in the lakes. The lakes are especially sensitive to changing catchment rainfall and have, in the past, ranged from near empty to much higher levels than today.
Kenya’s October to December 2019 rains were the highest on record for decades. These were followed by above-average rains in 2020. In some areas they were 400% more than normal.
With persistent rainfall, the catchment surface layers saturate, resulting in extended flood periods. For instance the Turkwel dam, which was built on the Turkwel river in the northern Rift Valley Basin, recently reached its highest level on record.
And in May this year, Lake Naivasha reached its highest level since 1932. The lake’s expansion has flooded developments, such as surrounding flower farms.
Yet, like the other lakes, Lake Naivasha’s waters have historically been higher. The lake is 1.4 vertical metres short of its official riparian boundary. In 1917, the lake was 2.4 metres higher. In earlier centuries, the lake was at least 13 metres higher.
The water cycles of Rift Valley lakes are changing as water is taken out for use and because the catchments and land surrounding the lakes are being degraded. For instance, forests are being converted into agricultural land, there is increasing urbanisation and people are encroaching onto riparian and wetland zones.
Lake Nakuru’s ecology has long been affected by catchment change. For instance, the forest cover of its catchment area is reported to have declined from 70% to 15% over the past 50 years, leading to greater runoff into rivers and thence to the lake. On top of that, the growth of Nakuru town requires more water supply which will be imported. Unless otherwise channelled, this extra water will end up in the lake, raising water levels, and if not properly treated, will worsen pollution.
Meanwhile, Lake Naivasha declined in recent years to critically low levels. Growing developments – such as Naivasha town and a new Industrial City – need water, which puts more pressure on the already critically stressed lake water resource. In addition, the lake suffers from heavy pollution loads.
The flow of water into Lake Turkana is being regulated by dam and irrigation developments, potentially affecting the lake ecology and fisheries.
Excessive river inflows into the lakes result from increasing catchment rainfall coupled with the effects of land use changes. Dilution of saline waters affects the production of cyanobacteria, the food sources of lesser flamingos. Increased turbidity reduces light penetration into water, and affects photosynthesis, an engine of the aquatic food chain.
While tectonic plate changes are beyond humans’ control, biodiversity-friendly land use and commitment to existing legislation and national vegetation cover goals can limit catastrophic damage to lake ecological systems, people and property.
In the context of increasing rainfall trends, it is vital that official demarcation of riparian and wetland zones takes full account of the very well-documented extreme high lake level precedents and extent of flooding of the last century and before.